Dust, volcanic ash, and the evolution of the South Pacific Gyre through the Cenozoic-Reference-Cited by-同舟云学术

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Dust, volcanic ash, and the evolution of the South Pacific Gyre through the Cenozoic

Published:2015-08 Issue:8 Volume:30 Page:1078-1099
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Dunlea Ann G.¹,Murray Richard W.¹,Sauvage Justine²,Spivack Arthur J.²,Harris Robert N.³,D'Hondt Steven²

Affiliation:

1. Department of Earth and Environment; Boston University; Boston Massachusetts USA

2. Graduate School of Oceanography; University of Rhode Island; Narragansett Rhode Island USA

3. College of Earth, Ocean, and Atmospheric Sciences; Oregon State University; Corvallis Oregon USA

Funder

U.S. National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference70 articles.

1. Cenozoic bathyal and abyssal ostracods beneath the oligotrophic South Pacific Gyre (IODP Expedition 329 Sites U1367, U1368 and U1370);Alvarez Zarikian;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2015

2. Metalliferous sediments from DSDP Leg 92: The East Pacific Rise transect;Barrett;Geochim. Cosmochim. Acta,1987

3. Eocene cooling linked to early flow across the Tasmanian Gateway;Bijl;Proc. Natl. Acad. Sci. U.S.A.,2013

4. Morphology and origin of the Osbourn Trough;Billen;J. Geophys. Res.,2000

5. Response of the ITCZ to Northern Hemisphere cooling;Broccoli;Geophys. Res. Lett.,2006

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